A towering ash plume, cascading debris, and steam explosions suggested that the eruption of Pavlof Volcano had intensified several days after it began. On May 16, 2013, the Alaska Volcano Observatory reported ash plumes reaching up to 12,000 feet (3,700 meters) above the volcano’s summit. The plumes were accompanied by lava fountains and a lava flow that descended the steep northern flank of the volcano.
This natural-color satellite image, collected by the Advanced Land Imager (ALI) on the Earth Observing-1 (EO-1) satellite, shows Pavlof on May 16, 2013. A brown ash plume blew from the summit towards the southeast, and gray ash from earlier explosions covered the snow on the volcano’s upper slopes. To the northeast, additional ash rose from an ongoing lava flow.
Explosive vaporization of snow by the hot lava and debris is likely converting a mild flow into a violent pyroclastic flow—an avalanche of extremely hot gas, ash, and volcanic rocks. Further to the northwest, rising steam and volcanic gases trace the path of the debris, a slushy mix of ash, rock fragments, ice, and water called a lahar. Additional debris from the flows left dark trails on Pavlof’s northern flank.
Located near the western end of the Alaska Peninsula, Pavlof isn’t a direct threat to any large cities or towns. However, ash from an eruption could disrupt air traffic from Asia to North America and Europe.
- Alaska Volcano Observatory (2013, May 16) Daily Update. Accessed May 17, 2013.
- Eruptions Blog (2013, May 16) Lava Flows and Ash Plume as Eruption Continues at Pavlof. Accessed May 17, 2013.
- INGV Sezione di Catania (2013, February 19) Etna and Stromboli Update. Accessed May 17, 2013.
- McNutt, S. R., et al, (1991, February) Geological and seismological evidence of increased explosivity during the 1986 eruptions of Pavlof volcano, Alaska. Bulletin of Volcanology, 53 (2), 86-98.
NASA Earth Observatory image by Jesse Allen and Robert Simmon, using EO-1 ALI data from the NASA EO-1 team. Caption by Robert Simmon, with input from Erik Klemetti (Denison University) and Dave Mayer (Clark University).
- EO-1 - ALI